Wood use in a medieval village: the contribution of wood charcoal analysis to the history of land use during the 13th and 14th centuries a.d. at Pobla d’Ifach, Calp, Alicante, Spain

Excavations on the Rock of Ifach, Alicante, Spain have revealed the remains of a medieval settlement that flourished between a.d. 1297 and 1359. Wood charcoal analysis combined with archaeological evidence and historical records allow an assessment of the local vegetation of the area during the medieval period, the obtaining and use of firewood and the commercial routes for supplying timber. Pinus halepensis and to a lesser degree various matorral taxa were used for fuel during the main occupation phases at the settlement. The resource exploitation network of the settlement expanded over the adjacent coastal area, with firewood obtained from pine woodlands there. The timbers used in the construction of the settlement were mainly from pines that originated nearby (P. halepensis) or which were transported by river from woodland areas to the north which were controlled by the Crown of Aragon (P. nigra/sylvestris, P. pinaster). The partial destruction of the village in a.d. 1359 and its gradual abandonment are reflected in changes observed in fuel supplying practices that then concentrated on the local matorral vegetation of the rock itself.     

Economy and environment of Bronze Age settlements – Terramaras – on the Po Plain (Northern Italy): first results from the archaeobotanical research at the Terramara di Montale

The paper presents a synthesis of the on-site archaeobotanical investigations of the Terramara di Montale, one of the most important sites of the Terramara cultural system which characterised the Po Plain in the Middle-Late Bronze Age (1650–1200 b.c.). Samples for pollen analysis and macroremains, including seed/fruit and wood/charcoal records, were collected from stratigraphic sequences and occupation levels during the excavations 1996–2001. The results permitted the reconstruction of the main characteristics of the landscape which at the onset of the Terramara rapidly passed from a natural, more forested landscape with mixed oak wood and conifers to a more open and anthropic landscape characterised by cereal fields, pastures and meadows. People felled oaks and other trees such as Populus/Salix and Fraxinus to make piles or walls for houses. Wood from these species was also recorded as charcoal in the hearths. Palynological and carpological data show that the inhabitants of the Terramara largely founded their economy on cereals (mainly Triticum aestivum/durum, T. dicoccum and Hordeum vulgare). They also grew a few legumes (Vicia faba var. minor, Vicia sp. and Lens culinaris). There was also grazing by domestic animals, mainly ovicaprines but also pigs and cattle, and these were fed exploiting wild plants such as Carpinus. In the paper the four main steps of the history of the Terramara are described (before the Terramara, the onset, the Terramara phase, the decline) during which both human influence and climatic changes were important. At the onset of the Terramara (around 1600 b.c.) a warm and possibly dry phase occurred. The intense use of the territory and a climatic deterioration at around 1300 b.c. might have triggered the decline of the Terramara di Montale.     

Vegetation change during the Bronze Age studied in a multi-proxy approach: use of wood linked to charcoal analysis

During recent archaeological excavations in the alpine valley of Montafon, western Austria, a Bronze and early Iron Age settlement cluster located at about 1,000 m a.s.l. was excavated. The human impact on the woodland resulting from these prehistoric settlement activities has been evaluated by the analysis of charred plant macro remains from cultural layers from a hilltop settlement site and two other close-by settlements, all of them encompassing the Early and Middle Bronze Age (19th to 15th century cal. b.c.) and early Iron Age (6th/5th century cal. b.c.). Charred seeds and fruits have provided information on the supply of foodstuff while charcoal (anthracological) analyses of firewood have revealed the use of wood and consequently the changes in local woods. The latter analyses suggest that the spruce-fir woodland (Piceeto-Abietetum) was gradually cleared from the Early Bronze Age. During the Middle Bronze Age large amounts of Pinus sylvestris (pine), Betula (birch), Corylus avellana (hazel) and Sorbus (rowan) with some Picea abies (spruce) characterized the woods, and early succession stages indicate clearings. These anthracological studies are corroborated by pollen studies disclosing clearings in the woods since the Early Bronze Age, which gradually expanded during the Middle Bronze Age. Furthermore, several charcoals from a Middle Bronze Age hearth seem to be of the same age, and the pattern of their annual growth-rings suggests the pollarding of broadleaved trees.     

Archaeological charcoals as archives for firewood preferences and vegetation composition during the late Holocene in the southern Mayumbe,Democratic Republic of the Congo (DRC)

Analysis of charcoal from an archaeological assemblage near the Lukula community located at the southernmost boundary of the Mayombe forest (Bas-Congo, DRC) yielded 30 taxa used as firewood between 1,200 and 700 cal. b.p. Local people mentioned 71 taxa preferred for use nowadays. The identified taxa belong either to mature rainforest, pioneer forest, regenerating forest or woodland savanna, indicating that ancient and current local populations gathered firewood in several different forest types. Modern firewood preferences do not seem to agree with the archaeobotanical composition. Also, linguistic evidence does not indicate a long exploitation history for all of the recorded taxa. Furthermore, no particular wood qualities such as wood density, calorific value or magical or medicinal properties seem to determine the Lukula assemblage, which was probably composed of waste material from various activities which required different specific firewood characteristics. As such, taxa composition is not biased by human selection, suggesting that it reflects the surrounding environment, which was characterised by mature rainforest with patches of regenerating forest and open vegetation types. Unlike the origin of present-day forest-savanna mosaics from human activity, fragmentation around 1,000 cal. b.p. may have been provoked by a well-known climatic event coinciding with the Medieval Climate Anomaly, which undoubtedly had a significant impact on Central African forest composition.     

Insight into the environment of a pre-Roman Iron Age hillfort at Vladař, Czech Republic, using a multi-proxy approach

The large fortified hilltop site of Vladař, northwest Bohemia, Czech Republic (50°05′N, 13°13′E), has recently been studied intensively by way of environmental archaeology, in which palaeoecological methods have played a crucial role. The latter include the analyses of pollen, green algae, Cladocera, other microfossils, plant macro-remains (including charcoal and wood) and chemical composition, carried out on the wet sediments from an artificial cistern/pond situated in the middle of the large citadel, supplemented by charcoal and wood analysis on material from dry situations. The continuous palaeoecological record consists of well-preserved biological remains and covers the period from ca. 400 b.c. to recent times. The chronology is primarily based on radiocarbon dating, supplemented by archaeological finds. The main focus is on the La Tène period of the Iron Age. During the early to middle La Tène the hillfort had a considerable number of permanent inhabitants and woodland was almost completely replaced by an agricultural landscape. The site became partly abandoned by the end of the 3rd century b.c. and completely abandoned around the birth of Christ, after which it reverted to natural woodland communities.     

Anthracological analysis from Kovacevo, southwest Bulgaria: woodland vegetation and its use during the earliest stages of the European Neolithic

Wood charcoal analysis from Kovacevo in southwest Bulgaria, one of the earliest Neolithic sites in southeastern Europe, provided information about the first stages of anthropogenic impact on vegetation during the Early Neolithic (6159–5630 cal b.c.). Deciduous oak was the most abundant and frequently used taxon in the wood charcoal assemblages. Cornus charcoal was also abundant, probably connected with the use of its twigs as building material in wattle and daub structures. The dominant deciduous oak forest was opened during the Kovacevo I period, as shown by evidence from the Kovacevo Ia and Kovacevo Ib occupation phases. Other types of vegetation, like Black pine (Pinus nigra) woodland, riverine forests and some sub-Mediterranean elements, were used only sporadically, indicating high and sustained availability of wood resources in the oak forests. Anthropogenic impacts were gradual, a pattern that matches contemporary studies elsewhere in the region.     

The availability and use of wood resources at the multi-period settlement site of Pyeonggeo-dong, Jinju, South Korea

Analysis of wood charcoal that was conducted as a part of an interdisciplinary project at Pyeonggeo-dong, a multi-period agricultural complex located in Jinju, South Korea, reveals oak (Quercus sp.) to be the most commonly encountered wood over the period of 4000–1500 cal. b.p. The charcoal data indicate that Quercus was one of the most abundant woody plants in the surrounding vegetation, although its dominance in the charcoal assemblage may partly represent preferential human selection in the past. The data suggest that Quercus-dominant forest declined with the growth of a secondary forest of Platycarya strobilacea around the site from about a.d. 300. This change postdates by more than a thousand years the earliest evidence of large-scale agriculture, which is visible in the form of carbonized crops and large tracts of prehistoric agricultural fields. A relatively large number of pit dwellings for the Three-Kingdoms period (ca. a.d. 300–500) at Pyeonggeo-dong suggests that this late sign of human impact on vegetation is related to the extension of agricultural fields to previously uncultivated hilly areas and/or increased needs for fuel and timber caused by high population density of the site.     

Charcoal production in the Mopane woodlands of Mozambique: what are the trade-offs with other ecosystem services?

African woodlands form a major part of the tropical grassy biome and support the livelihoods of millions of rural and urban people. Charcoal production in particular is a major economic activity, but its impact on other ecosystem services is little studied. To address this, our study collected biophysical and social datasets, which were combined in ecological production functions, to assess ecosystem service provision and its change under different charcoal production scenarios in Gaza Province, southern Mozambique. We found that villages with longer histories of charcoal production had experienced declines in wood suitable for charcoal, firewood and construction, and tended to have lower perceived availabilities of these services. Scenarios of future charcoal impacts indicated that firewood and woody construction services were likely to trade-off with charcoal production. However, even under the most extreme charcoal scenario, these services were not completely lost. Other provisioning services, such as wild food, medicinal plants and grass, were largely unaffected by charcoal production. To reduce the future impacts of charcoal production, producers must avoid increased intensification of charcoal extraction by avoiding the expansion of species and sizes of trees used for charcoal production. This is a major challenge to land managers and policymakers in the area.This article is part of the themed issue ‘Tropical grassy biomes: linking ecology, human use and conservation’.     

Grazing impacts and woodland management in Eriksfjord: Betula, coprophilous fungi and the Norse settlement of Greenland

This paper focuses on the impact of Norse settlement on vegetation and landscape around the head of Tunulliarfik (Eriksfjord) in southern Greenland. Pollen, radiocarbon, microscopic charcoal and fungal spore data are presented from a peat monolith which was collected close to the ruins of a large Norse farm complex (group ?39 at Qinngua in the former Eastern Settlement). Landnám is identified at ca. cal. a.d. 1020 by a small decrease in pollen from Betula, a slight increase in Poaceae, and the appearance of pollen from Norse apophytes (native plants favoured and spread by human activity) and anthropochores (not native and unintentionally introduced by people). Increases in microscopic charcoal and palynological richness are also apparent. This pattern is broadly consistent with that seen in other pollen diagrams from this region. The sequence is unusual for Greenland, however, in that relatively high Betula pollen percentages (average 20% TLP) are recorded throughout the period of settlement, up to the end of the 14th century a.d. before the profile becomes truncated. If these data are primarily representative of the dry land vegetation, then they suggest that birch woodland and scrub may well have persisted close to the farm throughout the Norse period. Given the potential resource value of woodland to the settlers, this may imply that birch was being managed sustainably, as was the case in Iceland during the medieval period. Coprophilous fungal spores typically found on animal dung are abundant during the early phase of settlement, yet subsequently decline in abundance. This may indicate a likely decrease in grazing intensity or livestock numbers over time, possibly in response to climatic deterioration and/or soil erosion that is expected to have placed increased stress on the pastoral farming system.     

Interpretation of charcoal and pollen data relating to a late Iron Age ritual site in eastern Ireland: a holistic approach

The study of charcoal produced by five burning episodes that occurred in a rapid succession within a ritual pit dating to the late Iron Age at Raffin Fort, Co. Meath, Ireland, reveals considerable variation in the charcoal assemblages resulting from each burning episode. Wood selection processes are considered against the background of information on woodland composition and land-use history provided by a detailed pollen diagram from nearby Emlagh Bog, the chronology of which is based on both AMS ¹⁴C dates and tephra analysis. A human skull fragment lay on top of the charcoal layers but the radiocarbon evidence indicates that the skull predated the burnings by at least a century. This and other evidence indicate a ritual pit with the skull as a human relic. It is suggested that, in this instance, wood selection was neither random nor determined solely by availability or combustibility, but instead may have been informed by socio-religious belief systems pertaining to trees and wood. Early Irish documentary sources, which reveal a complex ethnography of wood and trees in later prehistoric and early historic Ireland, are reviewed. The results shed fresh light on aspects of late Iron Age archaeology in a part of Europe that was outside the direct influence of the Roman world. New information is provided on a distinctive feature in late Holocene Irish pollen records namely the Late Iron Age Lull (ca. a.d. 1–500). During this time, widespread regeneration of woody vegetation took place. In the subsequent early Medieval period renewed farming activity resulted in substantial decline in woodland, a pattern also seen at many other locations in Ireland.     

The diet of Eneolithic (Copper Age, Fourth millennium cal b.c.) pile dwellers and the early formation of the cultural landscape south of the Alps: a case study from Slovenia

Analyses were performed of plant remains from the Late Neolithic (in Slovenian terminology corresponding to Eneolithic or Copper Age, ca. 4300–2300 b.c.) pile dwelling Hočevarica in the Ljubljansko barje (Ljubljana Moor), Slovenia. This settlement existed between ca. 3650 and 3550 cal b.c. Seeds, fruits, wooden piles, macroscopic charcoal and pollen from the cultural layers were analysed. The remains of domestic plants such as charred grains of Hordeum vulgare (barley), Triticum monococcum, T. dicoccum (einkorn and emmer wheat) and Papaver somniferum (poppy seeds), as well as seeds of weeds such as Chenopodium album-type indicate early cultivation in the area. In addition, numerous remains of nuts and berries, especially of Quercus sp., Cornus mas, Rubus fruticosus and Corylus avellana demonstrate that the gathering of wild plants was an important part of subsistence. Palaeoecological and archaeobotanical data from Hočevarica further suggest that cleared land was used for agriculture and pastures during the Neolithic, and that different wood was cut for construction and for fuel. The species assemblage from Hočevarica is very similar to those recovered from northern Alpine lake dwelling sites, however, several new taxa (e.g. Lathyrus sativus, Vicia sp.) appear in the assemblage. One of the most surprising finds is the seed of wild grape (Vitis vinifera ssp. sylvestris), which are the oldest on-site remains of grapevine from Slovenia.     

Hints of economic change during the late Roman Empire period in central Italy: a study of charred plant remains from “La Fontanaccia”, near Rome

The archaeobotanical study of the charred macro-remains recovered from the burnt settlement of La Fontanaccia, Allumiere, 50 km northwest of Rome, a small hut from the time of the end of the late Roman Empire, provided results on the use of food of its inhabitants, their living conditions, and the natural environment. The fire which destroyed the small settlement was archaeologically dated to the middle of the 5th century a.d., few years before the end of the Roman Empire. This was a period in which the state structure, undermined by the barbarian invasions which provoked famine and destruction, was in deep economic and political crisis, and the population in Rome and in the countryside lived in precarious conditions. No archaeo-botanical data have been available until now for this period in the region of Rome. The presence of grass peas, acorns, two-rowed barley caryopses, and small horse bean seeds demonstrate the general state of regression in the late Roman Empire, when misery and famine were widespread. The finds of charcoal from chestnut, deciduous oak, maple and elm suggest the presence of thermophilous deciduous woods and environmental conditions similar to today’s. It deserves mention that this is the first site in which macro-remains (charcoal) of Castanea have been found in central Italy.     

Four thousand years of plant exploitation in the Chad Basin of northeast Nigeria I: The archaeobotany of Kursakata

This paper discusses archaeobotanical remains from the settlement mound of Kursakata, Nigeria, comprising both charred and uncharred seeds and fruits as well as charcoal. In addition, impressions of plant tempering material in potsherds were analysed. The late Stone Age and Iron Age sequence at Kursakata is date from 1000 cal. B.C. to cal. A.D. 100. DomesticatedPennisetum (pearl millet), wild Paniceae and wild rice are the most common taxa. Kernels from tree fruits were regularly found including large numbers ofVitex simplicifolia—a tree which is absent from the area today. A distinct change in plant spectra can be observed between the late Stone Age and the Iron Age. Although domesticated pearl millet was already known at the beginning of the settlement sequence of Kursakata, it only gained greater economic importance during the Iron Age. Besides farming, pastoralism and fishing, gathering of wild plants always played a major role in the subsistence strategy of the inhabitants of Kursakata. The charcoal results show that firewood was mainly collected from woodlands on the clay plains, which must have been more diverse than today. The end of the late Stone Age in the Chad Basin was presumably accompanied by the onset of drier environmental conditions from ca. 800 cal. B.C. onwards.     

Archaeobotanical data and crop storage evidence from an early Bronze Age 2 burnt house at Arslantepe, Malatya, Turkey

Excavations on the southwest area at Arslantepe, Malatya, Turkey, by far the largest tell on the Malatya plain from the 5th millennium to the Neo-Hittite age, revealed an important change in the settlement patterns during the two main levels of the VI C Period of the site (Early Bronze Age 2, 2750–2500 cal b.c.). The latter level corresponds to a village founded on neatly shaped terraces in a layout which lasted for centuries, well into the following Early Bronze Age 3. This continuity was not broken even by violent fires that at times destroyed some houses, producing a huge quantity of charred plant remains, which comprised fruits, seeds and wood charcoal. The archaeobotanical data so far obtained from the EB2 house A607, the richest one in macro-remains, on which efforts have been concentrated first, provides much data about the use of the surrounding land. Charcoal of Quercus (deciduous oaks) (85%) followed by Populus (poplar) (9%) are dominant among wood remains, while Hordeum (barley) (70%) is the dominant crop found, followed by Cicer (chickpea) (17%). The crop storage methods were investigated by mapping the positions of charred fruits and seeds both according to the grid system and in comparison to the layout of facilities (grinding stone, hearths, oven) and the distribution of pottery (jars, bowls, pots) in order to detect where the crops were kept and the ways in which they were stored, processed, and used. The house facilities and furniture suggest that the house was a multifunctional place, which included storage space, but which was limited to household needs. The new archaeobotanical investigation so far carried out on the burnt house A607 suggests some implications on the degree of agriculture, on crop storage and on food processing practises and also gives information on the natural landscape surrounding the site.     

Étude des macro-, méso- et micro-charbons du site épigravettien de Mezhyrich (Ukraine) : données taphonomiques et anthracologiques

This paper is the state of the art of charcoal signal studies (macro-, meso- and micro-charcoal) that have been carried out at the Epigravettian settlement of Mezhyrich. This work took part of the French ANR project “Mammouths”. Charcoal signals have been found in both natural and archaeological (pits and activity areas) deposits that have been sampled during the 2007–2008 archaeological excavations. This study aims at discussing the natural versus anthropic causes of those charcoal signals. Microscopic charcoal have been observed and quantified from loess sediments; they are probably the consequence of regional fire regimes. Charcoal signals found in archaeological layers would be mainly caused by human activities. The major charcoal signal is observed within the microscopic part of the archaeological sediments and thereby underlines the intensity of taphonomic processes. The identification of wood charcoal shows that birch and willow were located along the riverbanks, which provides further discussion of prehistoric fuel management in Pleniglacial context.     

The impact of mining on the woody vegetation of the southern Andes: a study of charcoal from the Andean Precordillera in central western Argentina in the 18th and 19th centuries

Mining has played an important role in the generation of economic wealth since colonial times in South America. However, the impact of historical mining on the environment has not been studied in detail. In view of this, and based on the analysis of archaeological and modern wood data, we discuss the impact of historical mining and human occupation on the woody vegetation of an arid region in the southern Andes. We present the results of the analysis of archaeobotanical charcoal remains recovered from the “Los Hornillos” mining site located in the Andean Precordillera, northwestern Mendoza Province, Argentina. The archaeobotanical materials date from the late 18th to the early 19th century. Based upon wood anatomy, 60% of charcoal fragments were associated with Adesmia cf. uspallatensis, a shrub widely distributed there. We assessed the impact and legacy of human occupation on local and regional plant communities based on charcoal evidence, archaeological data and the age of living A. uspallatensis shrubs growing around the mining site. This analysis allowed us to determine the rate of growth of this species (1.22 mm per year) and mean maximum ages of around 70 years. Therefore, the current development of woody communities in this area is thought to be representative of recovery after historical mining and occupation across the Andean Precordillera and suggests that obtaining firewood for mining activities constituted an important factor influencing past natural vegetation dynamics.

     

Biogas plants for small farms in Kenya

This paper reports on the authors' efforts to improve the small farm community welfare in Kenya by promoting biogas technology. The survey showed that fuel was used in Kenyan farms mainly for cooking and lighting, and wood, crop residue, and charcoal were the predominant fuel sources. Mostly women collected firewood, fetched water, and cooked. Building a fire with these fuels was time-consuming, and smoke from these fires was damaging to the living environment. Hence, applying biogas technology to Kenyan small farms not only guarantees a reliable, renewable energy source, but also provides other benefits, such as cleaner household environments, better working conditions for housewives,     

Plant subsistence and environment at the Mesolithic site T?gerup, southern Sweden: new insights on the “Nut Age”

Pollen was analysed from a sediment sequence collected in the close vicinity of the Mesolithic settlement T?gerup, southern Sweden. Macroremains were also retrieved from numerous samples taken at the site of the archaeological excavations of Kongemose and Erteb?lle settlement phases, 6700–6000 b.c. and 5500–4900 b.c. respectively. Plants and other organic remains were well preserved in the refuse layers from the settlements embedded in the gyttja. The pollen record includes no clear indications of human impact on the vegetation during the Mesolithic. The occurrence of charcoal particles and pollen of grass and herbs associated with nutrient-rich soils are contemporaneous with the Kongemose settlement. The Erteb?lle settlement phase, although characterised by considerable dwelling activities less than a hundred metres from the pollen sampling site, is scarcely seen in the pollen data. Numerous finds of crushed dogwood stones from the Kongemose phase, often partly carbonised, suggest that these stones were used for the extraction of oil. Other plants found in the Kongemose refuse layers that may have been used are apples, cherries, raspberries, acorns and rowan-berries. Based on the abundance of hazelnut shells found at the studied site and in other studies of Mesolithic sites in southern Scandinavia it is proposed that these remains may testify to an important food supply rather than just use as a supplement to animal protein. It is also hypothesised that a regional decrease in hazel populations and thus hazelnut availability at the end of the Mesolithic may have motivated the adoption of Neolithic subsistence.     

Plant macrofossils from the Roman settlement of Terronha de Pinhovelo, northwest Iberia

Several samples were collected during the archaeological excavations at the proto-historic and Roman settlement of Terronha de Pinhovelo, northeast Portugal, in order to obtain plant macrofossils. The relevant archaeobotanical data gathered from the Roman structures of Sector B at the site allow a further understanding of the settlement and its community’s daily life between the 4th and 5th centuries a.d. In the charcoal analysis, the main types recovered were Pinus pinaster, Quercus pyrenaica type, Q. faginea type, Q. suber type, Arbutus unedo and Fraxinus angustifolia. The shrubs, significantly less abundant in the samples, were represented by Cistus sp., Leguminosae and Erica spp. It must be stressed that the samples were taken from well-delimited domestic hearths and the botanical remains result from specific choices of firewood in short episodes of time, and therefore not the most appropriate for palaeoecological approaches, which usually cover a longer time span. The cereals are the most frequent group of plants represented in the fruit and seed assemblages. Triticum aestivum/durum, T. compactum, T. spelta and Hordeum vulgare were the dominant crops, followed by T. dicoccum and Panicum miliaceum. The only pulse identified was Vicia faba var. minor, in quite abundant quantity although it came almost exclusively from just one hearth. Two of the compartments sampled seem to be directly connected to plant processing, but the presence together of several plant taxa in the domestic structures makes their understanding quite difficult. These palaeoeconomic data are consistent with the records already available for northwest Iberia, and are significantly representative of a regular Romanised rural community.     

Vegetation stability in the Southeastern Brazilian coastal area from 5500 to 1400 14C yr BP deduced from charcoal analysis

Charcoal analysis of six shell mounds showed that no major changes of the mainland vegetation ecosystem have taken place along the southeastern Brazilian coast (22 degrees 53'-22 degrees 57'S, 42 degrees 03'-42 degrees 33'W) from 5500 to 1400 14C yr BP. These shell mounds have been occupied by sedentary fisher-gatherer-hunters. Charcoal fragments retrieved from vertical profiles in the archaeological sites were examined; taxonomic determinations were based on a reference collection of charred woods and a program for computer-aided identification. Charcoal assemblages of all the studied sites present taxa from various restinga vegetation types, mangroves, xeromorphic coastal forest, and inland Atlantic Forest. The restinga ecosystem, characteristic of the Brazilian coast, is associated with sandy beach ridges; the restinga forest was much more abundant during the studied period than nowadays. The charcoal assemblages represent mainly the local vegetation; a regional reconstruction depends on the study of numerous sites. In the Cabo Frio region, open restinga taxa are more abundant in the Sambaqui do Forte, while forest elements are more important in the Sambaquis Salinas Peroano and Boca da Barra. The sites studied in the Arraial do Cabo (Sambaqui da Ponta da Cabe?a) and in the Saquarema regions (Sambaquis da Pontinha and da Beirada) show that open restinga formations were locally predominant. A comparison of multivariate analysis applied to both charcoal assemblages and to phytosociological data of the extant vegetation showed a good correspondence between the charcoal spectra and the present vegetation. The high taxonomic diversity of archaeological charcoal samples and numerous fragments showing traces of decay before charring suggests that aleatory gathering of dead wood constituted the main source of firewood for fisher-gatherer-hunters populations. Condalia sp. was probably selected for cultural reasons.The only significant fluctuations on the charcoal spectra relate to the mangrove vegetation. Two relatively humid episodes (recorded from ca. 5500 to 4900/4500 and from ca. 2300 to 2000 14C yr BP), intercalated by two episodes of increased dryness with increased lagoon salinity (from ca. 4900/4500 to 2300 and from ca. 2000 to 1400 14C yr BP) were recorded in the Cabo Frio region. The changes in mangrove vegetation cannot be attributed to sea-level variations, for the three regressive and the two transgressive episodes identified for the Brazilian coast during this period are not in phase with the development of mangroves. The stability of the mainland vegetation ecosystem is probably due to the edaphic character of the coastal environments, which makes coastal formations much more resistant to climatic variations and less sensitive to climatic change. We propose that this environmental stability was a decisive factor in the maintenance of the fisher-gatherer-hunter sociocultural system.